Synchronous Periadriatic magmatism in the Western and Central Alps in the absence of slab breakoff

Periadriatic Alpine magmatism has long been attributed to slab breakoff after Adria–Europe continental collision, but this interpretation is challenged by geophysical data suggesting the existence of a continuous slab. Here, we shed light on this issue based on a comprehensive dataset of zircon U–Pb...

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Veröffentlicht in:	Terra nova (Oxford, England) England), 2019-04, Vol.31 (2), p.120-128
Hauptverfasser:	Ji, Wei‐Qiang, Malusà, Marco G., Tiepolo, Massimo, Langone, Antonio, Zhao, Liang, Wu, Fu‐Yuan
Format:	Artikel
Sprache:	eng
Schlagworte:	Eocene Geophysical data Isotopes Magma Oligocene Subduction Zircon
Online-Zugang:	Volltext
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